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  2. Spruce Pine Mining District - Wikipedia

    en.wikipedia.org/wiki/Spruce_Pine_Mining_District

    Spruce Pine district is one of the largest suppliers of high-purity quartz, which is used in the manufacture of silicon for integrated circuits. [2] The district is named after the town of Spruce Pine , which is located in the middle of the region and is the hub of major mining activity there.

  3. Cambria (company) - Wikipedia

    en.wikipedia.org/wiki/Cambria_(company)

    A silo, located on US 169 between St. Peter and Le Sueur, is rented by Cambria to store quartz granules and slabs. [13] The silo was repainted with the Cambria logo. Cambria was ordered to remove the sign by MnDOT because it violated state law against advertisements along public highway corridors and county ordinance in historic preservation districts. [13]

  4. Quartzite - Wikipedia

    en.wikipedia.org/wiki/Quartzite

    Quartzite can have a grainy, glassy, sandpaper-like surface. Quartzite is a hard, non-foliated metamorphic rock which was originally pure quartz sandstone. [1] [2] Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts.

  5. List of largest monoliths - Wikipedia

    en.wikipedia.org/wiki/List_of_largest_monoliths

    Monolith with bull, fox, and crane in low relief at Göbekli Tepe. The density of most stone is between 2 and 3 tons per cubic meter. Basalt weighs about 2.8 to 3.0 tons per cubic meter; granite averages about 2.75 metric tons per cubic meter; limestone, 2.7 metric tons per cubic meter; sandstone or marble, 2.5 tons per cubic meter.

  6. The must-see documentaries of 2024 - AOL

    www.aol.com/must-see-documentaries-2024...

    In a year in which it seemed every great luminary got a moment under the documentary lens, it can be a bit difficult to parse out which were must-see. This list will have you covered.

  7. Dynamic quartz recrystallization - Wikipedia

    en.wikipedia.org/wiki/Dynamic_quartz_re...

    The highest temperature of the three textures, grain boundary migration becomes the dominant mechanism at ~500-550°C. Exhibiting much larger recrystallized grain sizes than the other two regimes, in addition to lobate and highly interfingering boundaries, at these temperatures quartz is completely recrystallized.

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